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15. | | BATISTA, E. R.; RAMOS, N. P.; LUCHIARI JUNIOR, A. Bioeletricidade, mercado de carbono e o setor sucroalcooleiro paulista. In: STAB: Açúcar, álcool e subprodutos, v.27, n.2, p.32, 2008. Reumos do 9. Congresso Nacional da STAB, 2008, Maceió. Biblioteca(s): Embrapa Meio Ambiente. |
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Registro Completo
Biblioteca(s): |
Embrapa Cerrados. |
Data corrente: |
11/02/1993 |
Data da última atualização: |
23/04/1999 |
Autoria: |
LUCHIARI JUNIOR, A. |
Título: |
Measurements and predictions of evapotranspiration rates from irrigated wheat in the cerrados region of central Brazil. |
Ano de publicação: |
1988 |
Fonte/Imprenta: |
Ithaca: Cornell University, 1988. |
Páginas: |
171p. |
Idioma: |
Inglês |
Notas: |
Tese Doutorado. |
Conteúdo: |
The purpose of this study was to characterize evapotranspiration for irrigated wheat growing in the Cerrados Region of Central Brazil and to evaluate and test various methods for predicting evapotranspiration. Bowen ratio measurements were made on an hourly basis over irrigated wheat crops grown in the dry seasons of 1982 and 1983. This data was analyzed in order to evaluate factors affecting crop evapotranspiration and also was compared to rates of evapotranspiration predicted using the Priestley-Taylor equation and Monteith combination model. By comparing measured evapotranspiration to net radiation it was shown that sensible heat advection, for local and regional origin, can significantly affect crop water requirements in this region. The prortionality constant in the Prestley-Taylor equation had an average value of 1.2 for potential conditions under non-advective conditions and decrease gradually between irrigations. For irrigation management purposes the use of a value of 1.5 was seemed appropriate. Bulk canopy resistance required in the Monteith combination model was calculated using the energy balance method and the resindual method. Both methods produced comparable results and indicated that this resistance varied within well defined limits dictated by irrigation timing. When the combination model was used to predict crop evapotranspiration, results were in good agreement with those obtained from energy balance measurements. In calculating the aerodynamic resistance it was found that the effects of stability could be ignored. Also crop surface temperature predicted from measurements of wind speed and air temperature at one height above the canopy were in good agreement with infrared measured canopy temperarure. In order to evaluate the supply function for models predicting water movement in the soil-plant-atmosphere continuum the Libardi and Campbell methods for estimating soil hydraulic conductivity as a function of water content were compared. They produced similar results. The parametes required in Campbell's method could be obtained from routine soil characterization data, but field saturated hydraulic conductivity and field saturated water content must be known. Measured and predicted daily evapotranspiration rates and soil water potential at the upper 10cm soil-layer were in good agreement when the Monteith combination model was used as a demand function in a single-layer canopy and multi-layer soil model (GAPS). Predictions of hourly energy fluxes using a multi-layer canopy and multi-layer soil model (Cupid) were in good agreement with measured energy fluxes. MenosThe purpose of this study was to characterize evapotranspiration for irrigated wheat growing in the Cerrados Region of Central Brazil and to evaluate and test various methods for predicting evapotranspiration. Bowen ratio measurements were made on an hourly basis over irrigated wheat crops grown in the dry seasons of 1982 and 1983. This data was analyzed in order to evaluate factors affecting crop evapotranspiration and also was compared to rates of evapotranspiration predicted using the Priestley-Taylor equation and Monteith combination model. By comparing measured evapotranspiration to net radiation it was shown that sensible heat advection, for local and regional origin, can significantly affect crop water requirements in this region. The prortionality constant in the Prestley-Taylor equation had an average value of 1.2 for potential conditions under non-advective conditions and decrease gradually between irrigations. For irrigation management purposes the use of a value of 1.5 was seemed appropriate. Bulk canopy resistance required in the Monteith combination model was calculated using the energy balance method and the resindual method. Both methods produced comparable results and indicated that this resistance varied within well defined limits dictated by irrigation timing. When the combination model was used to predict crop evapotranspiration, results were in good agreement with those obtained from energy balance measurements. In calculating the aerodynamic resistance ... Mostrar Tudo |
Palavras-Chave: |
Brasil; Epoca seca; Medida; Regiao Central; Wheats. |
Thesagro: |
Cerrado; Cultura Irrigada; Evapotranspiração; Irrigação; Manejo; Solo; Trigo; Triticum Aestivum. |
Thesaurus NAL: |
evapotranspiration; irrigation. |
Categoria do assunto: |
-- |
Marc: |
LEADER 03444nam a2200313 a 4500 001 1563329 005 1999-04-23 008 1988 bl uuuu m 00u1 u #d 100 1 $aLUCHIARI JUNIOR, A. 245 $aMeasurements and predictions of evapotranspiration rates from irrigated wheat in the cerrados region of central Brazil. 260 $aIthaca: Cornell University$c1988 300 $a171p. 500 $aTese Doutorado. 520 $aThe purpose of this study was to characterize evapotranspiration for irrigated wheat growing in the Cerrados Region of Central Brazil and to evaluate and test various methods for predicting evapotranspiration. Bowen ratio measurements were made on an hourly basis over irrigated wheat crops grown in the dry seasons of 1982 and 1983. This data was analyzed in order to evaluate factors affecting crop evapotranspiration and also was compared to rates of evapotranspiration predicted using the Priestley-Taylor equation and Monteith combination model. By comparing measured evapotranspiration to net radiation it was shown that sensible heat advection, for local and regional origin, can significantly affect crop water requirements in this region. The prortionality constant in the Prestley-Taylor equation had an average value of 1.2 for potential conditions under non-advective conditions and decrease gradually between irrigations. For irrigation management purposes the use of a value of 1.5 was seemed appropriate. Bulk canopy resistance required in the Monteith combination model was calculated using the energy balance method and the resindual method. Both methods produced comparable results and indicated that this resistance varied within well defined limits dictated by irrigation timing. When the combination model was used to predict crop evapotranspiration, results were in good agreement with those obtained from energy balance measurements. In calculating the aerodynamic resistance it was found that the effects of stability could be ignored. Also crop surface temperature predicted from measurements of wind speed and air temperature at one height above the canopy were in good agreement with infrared measured canopy temperarure. In order to evaluate the supply function for models predicting water movement in the soil-plant-atmosphere continuum the Libardi and Campbell methods for estimating soil hydraulic conductivity as a function of water content were compared. They produced similar results. The parametes required in Campbell's method could be obtained from routine soil characterization data, but field saturated hydraulic conductivity and field saturated water content must be known. Measured and predicted daily evapotranspiration rates and soil water potential at the upper 10cm soil-layer were in good agreement when the Monteith combination model was used as a demand function in a single-layer canopy and multi-layer soil model (GAPS). Predictions of hourly energy fluxes using a multi-layer canopy and multi-layer soil model (Cupid) were in good agreement with measured energy fluxes. 650 $aevapotranspiration 650 $airrigation 650 $aCerrado 650 $aCultura Irrigada 650 $aEvapotranspiração 650 $aIrrigação 650 $aManejo 650 $aSolo 650 $aTrigo 650 $aTriticum Aestivum 653 $aBrasil 653 $aEpoca seca 653 $aMedida 653 $aRegiao Central 653 $aWheats
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